Climatic variability in Princess Elizabeth Land (East Antarctica) over the last 350 years
- 1. Institute of Earth Sciences, Saint Petersburg State University, St Petersburg (Russian Federation)
- 2. Arctic and Antarctic Res Inst, Climate and Environm Res Lab, St Petersburg (Russian Federation)
- 3. Laboratoire des Sciences du Climat et de l'Environnement - IPSL, UMR 8212, CEA-CNRS-UVSQ-Universite Paris Saclay, Gif-sur-Yvette (France)
Description
We use isotopic composition (δ D) data from six sites in Princess Elizabeth Land (PEL) in order to reconstruct air temperature variability in this sector of East Antarctica over the last 350 years. First, we use the present-day instrumental mean annual surface air temperature data to demonstrate that the studied region (between Russia's Progress, Vostok and Mirny research stations) is characterized by uniform temperature variability. We thus construct a stacked record of the temperature anomaly for the whole sector for the period of 1958-2015. A comparison of this series with the Southern Hemisphere climatic indices shows that the short-term inter-annual temperature variability is primarily governed by the Antarctic Oscillation (AAO) and Inter-decadal Pacific Oscillation (IPO) modes of atmospheric variability. However, the low-frequency temperature variability (with period > 27 years) is mainly related to the anomalies of the Indian Ocean Dipole (IOD) mode. We then construct a stacked record of δ D for the PEL for the period of 1654-2009 from individual normalized and filtered isotopic records obtained at six different sites ('PEL2016' stacked record). We use a linear regression of this record and the stacked PEL temperature record (with an apparent slope of 9 ± 5.4 parts per thousand degrees C-1) to convert PEL2016 into a temperature scale. Analysis of PEL2016 shows a 1 ± 0.6 degrees C warming in this region over the last 3 centuries, with a particularly cold period from the mid-18. to the mid-19. century. A peak of cooling occurred in the 1840's - a feature previously observed in other Antarctic records. We reveal that PEL2016 correlates with a low-frequency component of IOD and suggest that the IOD mode influences the Antarctic climate by modulating the activity of cyclones that bring heat and moisture to Antarctica. We also compare PEL2016 with other Antarctic stacked isotopic records. This work is a contribution to the PAGES (Past Global Changes) and IPICS (International Partnerships in Ice Core Sciences) Antarctica 2k projects. (authors)
Availability note (English)
Available from doi: http://dx.doi.org/10.5194/cp-13-61-2017Additional details
Identifiers
Publishing Information
- Journal Title
- Climate of the Past
- Journal Volume
- 13
- Journal Issue
- no.1
- Journal Page Range
- p. 61-71
- ISSN
- 1814-9324
INIS
- Country of Publication
- Germany
- Country of Input or Organization
- France
- INIS RN
- 53077871
- Subject category
- S54: ENVIRONMENTAL SCIENCES; S58: GEOSCIENCES;
- Descriptors DEI
- ANTARCTICA; CLIMATIC CHANGE; CYCLONES; DIPOLES; HEAT; HUMIDITY; INDIAN OCEAN; ISOTOPE RATIO; RUSSIAN FEDERATION; SOUTHERN HEMISPHERE; SOUTHERN OSCILLATION; SURFACE AIR; VARIATIONS
- Descriptors DEC
- AIR; ANTARCTIC REGIONS; CRYOSPHERE; DIMENSIONLESS NUMBERS; EARTH PLANET; EASTERN EUROPE; ENERGY; EUROPE; FLUIDS; GASES; MOISTURE; MULTIPOLES; PLANETS; POLAR REGIONS; SEAS; SURFACE WATERS